首次对比分析了EKB和MAGW ISTP SB RAS雷达数据中流星回波和自学习神经网络识别的零星散射

O. Berngardt
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引用次数: 0

摘要

本文介绍了ISTP SB RAS十米相干散射雷达接收信号自动分类算法的当前版本(v.1.1)。该算法是一种自学习神经网络,利用雷达数据和国际电离层和地磁场参考模型,从无线电波传播的物理建模结果中确定散射信号的类型。根据2021年的MAGW和EKB ISTP SB RAS雷达数据,该算法根据无线电波传播的物理解释参数和雷达测量的数据,自我学习将散射信号分类为最初未知的类别,识别出20个可能的隐藏类别中有15个经常观察到,其中14个可以从物理角度解释。为了演示该算法的操作,我们首次对该算法分配的信号观测进行了统计分析,我们将其分别解释为流星轨迹散射和零星E层散射。通过对2021-2022年EKB和MAGW雷达数据的统计分析,论证了这两种类型信号的距离-高度特征。在这两类的每小时平均观测次数之间,以及在这两类的每小时平均视距速度之间,都显示出一种相关性。所获得的结果可以分别解释为流星回波和零星散射,并可以利用雷达数据研究中性大气(从流星散射数据研究)和下层电离层(从零星散射观测研究)之间的相互作用。目前,该分类算法工作在自动模式下的ISTP SB RAS雷达上。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
The first comparative analysis of meteor echo and sporadic scattering identified by a self-learned neural network in EKB and MAGW ISTP SB RAS radar data
The paper describes the current version (v.1.1) of the algorithm for automatic classification of signals received by ISTP SB RAS decameter coherent scatter radars. The algorithm is a self-learning neural network that determines the type of scattered signals from the results of physical modeling of radio wave propagation, using radar data and international reference models of the ionosphere and geomagnetic field. According to MAGW and EKB ISTP SB RAS radar data for 2021, the algorithm self-learns to classify scattered signals into initially unknown classes based on physically interpreted parameters of radio wave propagation and data measured by the radar, with 15 frequently observed out of 20 possible hidden classes identified, 14 of which can be interpreted from a physical point of view. To demonstrate the operation of the algorithm, we present the first statistical analysis of observations of signals assigned by the algorithm to classes which we interpret as scattering by meteor trails and scattering with the sporadic E layer respectively. Through a statistical analysis of EKB and MAGW radar data during 2021–2022, we demonstrate the range-altitude characteristics of signals of these types. A correlation is shown between the hourly average numbers of observations of both classes, as well as between the hourly average line-of-sight velocities obtained for both classes. The results obtained make it possible to interpret these classes as a meteor echo and sporadic scattering respectively, and to use radar data to study the interaction between the neutral atmosphere (studied from meteor scattering data) and the lower ionosphere (studied from observations of sporadic scattering). Currently, this classification algorithm works in ISTP SB RAS radars in automatic mode.
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